Cargando…

How does the Earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet?

The Earth's chemical composition far from chemical equilibrium is unique in our Solar System, and this uniqueness has been attributed to the presence of widespread life on the planet. Here, I show how this notion can be quantified using non-equilibrium thermodynamics. Generating and maintaining...

Descripción completa

Detalles Bibliográficos
Autor principal: Kleidon, Axel
Formato: Online Artículo Texto
Lenguaje:English
Publicado: The Royal Society Publishing 2012
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3261436/
https://www.ncbi.nlm.nih.gov/pubmed/22291221
http://dx.doi.org/10.1098/rsta.2011.0316
_version_ 1782221594849968128
author Kleidon, Axel
author_facet Kleidon, Axel
author_sort Kleidon, Axel
collection PubMed
description The Earth's chemical composition far from chemical equilibrium is unique in our Solar System, and this uniqueness has been attributed to the presence of widespread life on the planet. Here, I show how this notion can be quantified using non-equilibrium thermodynamics. Generating and maintaining disequilibrium in a thermodynamic variable requires the extraction of power from another thermodynamic gradient, and the second law of thermodynamics imposes fundamental limits on how much power can be extracted. With this approach and associated limits, I show that the ability of abiotic processes to generate geochemical free energy that can be used to transform the surface–atmosphere environment is strongly limited to less than 1 TW. Photosynthetic life generates more than 200 TW by performing photochemistry, thereby substantiating the notion that a geochemical composition far from equilibrium can be a sign for strong biotic activity. Present-day free energy consumption by human activity in the form of industrial activity and human appropriated net primary productivity is of the order of 50 TW and therefore constitutes a considerable term in the free energy budget of the planet. When aiming to predict the future of the planet, we first note that since global changes are closely related to this consumption of free energy, and the demands for free energy by human activity are anticipated to increase substantially in the future, the central question in the context of predicting future global change is then how human free energy demands can increase sustainably without negatively impacting the ability of the Earth system to generate free energy. This question could be evaluated with climate models, and the potential deficiencies in these models to adequately represent the thermodynamics of the Earth system are discussed. Then, I illustrate the implications of this thermodynamic perspective by discussing the forms of renewable energy and planetary engineering that would enhance the overall free energy generation and, thereby ‘empower’ the future of the planet.
format Online
Article
Text
id pubmed-3261436
institution National Center for Biotechnology Information
language English
publishDate 2012
publisher The Royal Society Publishing
record_format MEDLINE/PubMed
spelling pubmed-32614362012-03-13 How does the Earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet? Kleidon, Axel Philos Trans A Math Phys Eng Sci Articles The Earth's chemical composition far from chemical equilibrium is unique in our Solar System, and this uniqueness has been attributed to the presence of widespread life on the planet. Here, I show how this notion can be quantified using non-equilibrium thermodynamics. Generating and maintaining disequilibrium in a thermodynamic variable requires the extraction of power from another thermodynamic gradient, and the second law of thermodynamics imposes fundamental limits on how much power can be extracted. With this approach and associated limits, I show that the ability of abiotic processes to generate geochemical free energy that can be used to transform the surface–atmosphere environment is strongly limited to less than 1 TW. Photosynthetic life generates more than 200 TW by performing photochemistry, thereby substantiating the notion that a geochemical composition far from equilibrium can be a sign for strong biotic activity. Present-day free energy consumption by human activity in the form of industrial activity and human appropriated net primary productivity is of the order of 50 TW and therefore constitutes a considerable term in the free energy budget of the planet. When aiming to predict the future of the planet, we first note that since global changes are closely related to this consumption of free energy, and the demands for free energy by human activity are anticipated to increase substantially in the future, the central question in the context of predicting future global change is then how human free energy demands can increase sustainably without negatively impacting the ability of the Earth system to generate free energy. This question could be evaluated with climate models, and the potential deficiencies in these models to adequately represent the thermodynamics of the Earth system are discussed. Then, I illustrate the implications of this thermodynamic perspective by discussing the forms of renewable energy and planetary engineering that would enhance the overall free energy generation and, thereby ‘empower’ the future of the planet. The Royal Society Publishing 2012-03-13 /pmc/articles/PMC3261436/ /pubmed/22291221 http://dx.doi.org/10.1098/rsta.2011.0316 Text en This journal is © 2012 The Royal Society http://creativecommons.org/licenses/by/3.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
spellingShingle Articles
Kleidon, Axel
How does the Earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet?
title How does the Earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet?
title_full How does the Earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet?
title_fullStr How does the Earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet?
title_full_unstemmed How does the Earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet?
title_short How does the Earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet?
title_sort how does the earth system generate and maintain thermodynamic disequilibrium and what does it imply for the future of the planet?
topic Articles
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3261436/
https://www.ncbi.nlm.nih.gov/pubmed/22291221
http://dx.doi.org/10.1098/rsta.2011.0316
work_keys_str_mv AT kleidonaxel howdoestheearthsystemgenerateandmaintainthermodynamicdisequilibriumandwhatdoesitimplyforthefutureoftheplanet